A non-linear velocity inversion of a moderately difficult synthetic model in a cross-hole geometry using ray trace tomography , by Christof Stork

The cross-hole transmission velocity inversion problem has a significant non-linear component because horizontal geology can radically effect horizontally traveling energy. the repeated application of a travel time linear inversion to reconstruct a sample cross-hole model is generally successful at removing these non-linear effects, but not entirely. Further improvement of the model seems to require that wave form amplitude and dispersion information be included in the inversion. Analysis of the wave forms for the sample model used here indicates that although the inversions are close to the original model, they are not close enough to be within the region of validity for Born inversion schemes.


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